File:CN24FG3.jpg
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Dark field transmission electron micrograph of a calcium dolomite (Ca1.12Mg0.88(CO2)x) of Eocene age. The prominent modulated structure is typical of sedimentary dolomite, and such crystals are metastable with respect to ideal stoichiometric dolomite. Photograph by Richard Reeder. From Land, Lyndon S., 1982, Dolomitization: AAPG Course Notes 24, p. 1-20.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:47, 15 July 2015 | | 496 × 611 (128 KB) | Molyneux (talk | contribs) | Dark field transmission electron micrograph of a calcium dolomite (Ca1.12Mg0.88(CO2)x) of Eocene age. The prominent modulated structure is typical of sedimentary dolomite, and such crystals are metastable with respect to ideal stoichiometric dolomite. ... |
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